The right dip in the graph is the path of the stream where pooling is occurring. The left dip is where sedimentation is occurring. Sand and gravel is building up beside the water and eventually decreasing in elevation as it reaches the bottom of bank.
The right dip in the graph is the path of the stream where pooling is occurring. The left dip is where sedimentation is occurring. Sand and gravel is building up beside the water and eventually decreasing in elevation as it reaches the bottom of bank.
Long Island B Flow Survey
*Measurements are in cubic feet per second
Flow was the heaviest just after the rainstorm on 6/12 and decreased gradually over sampling dates.
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